桂东南马山杂岩体地球化学与锆石U-Pb同位素年代学特征及其地质意义
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摘要
<正>华南地区在中生代以广泛分布基性-中酸性侵入岩和火山岩为特征,这些岩浆岩中以酸性的花岗岩和流纹岩为主,少量的玄武岩和中性岩,且花岗岩岩体常伴有成矿作用。华南中生代岩浆岩形成的构造背景一直是争论的焦点,李献华等(1999,2000,2001)在桂东南和粤西地区厘定出了一条北东向展布的钾玄质侵入岩带,包括广西横县的马山岩体、桂平的西山岩体、陆川县和广东化州县交界的清湖岩体等。钾玄质岩石主要起源于与俯冲作用
引文
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